Pamukkale, Cotton Castle
Located in southwestern Turkey, the hot springs of Pamukkale are a marvel of nature and are now a protected UNESCO World Heritage Site. The springs form a series of white limestone cascades that carpet the slope of the River Menderes valley.
Pamukkale means ‘Cotton Castle’ in Turkish. It lies in a fault zone, where two plates of the Earth’s crust meet. Tectonic movements in the area often cause earthquakes. They are also responsible for the creation of countless hot springs. The waters of Pamukkale hot springs are loaded with calcium and dissolved carbon dioxide, and these combine to form crystals of calcite, which precipitate out. Over time these crystals have built up to form limestone sheets. In some places these sheets appear to flow down the slope torrents, like rivers of frozen water. In others, the crystals have created forests of calcite stalactites and flooded terraces connected by spectacular limestone waterfalls.
The waters of Pamukkale’s hot springs gush out of the ground at a rate of 240 litres per second and have a temperature of 35˚C (95˚F). They are rich in dissolved calcium and carbon dioxide and contain very few impurities. As they cool, the calcite that precipitates out of them is dazzling white. Beneath the top layer of calcite visible are other, more ochre-coloured layers. These were laid down in the past when the spring waters were not pure. 5 kilometres (3.1 miles) from Pamukkale is Karahayit, which also has hot springs. Here, the water emerges at 38˚C and is loaded with iron, resulting in the formation of red limestone.
~ JM
Image Credit: http://bit.ly/1xJ6BTE
More Info: Pamukkale: http://bit.ly/1OKjHFm
Pamukkale Water Terraces: http://bit.ly/1BENndX
Soothing waters of Pamukkale: http://wxch.nl/1HULAss